Mantle convection: Revision history

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15 December 2023

  • curprev 02:5002:50, 15 December 2023‎ Ai talk contribs‎ 3,976 bytes +3,976‎ Created page with "== Introduction == Mantle convection is the slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior of the Earth to the surface. It is a key process that drives plate tectonics; the thermal convection in the mantle propels the movement of the lithospheric plates on the Earth's surface. Image:Detail-51355.jpg|thumb|center|A cross-section of the Earth showing the mantle convection currents...."
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